Uppermost crustal structure regulates the flow of the Greenland Ice Sheet
Abstract The flow of the Greenland Ice Sheet is controlled by subglacial processes and conditions that depend on the geological provenance and temperature of the crust beneath it, neither of which are adequately known. Here we present a seismic velocity model of the uppermost 5 km of the Greenlandic...
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2021
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Online Access: | http://dx.doi.org/10.1038/s41467-021-27537-5 https://www.nature.com/articles/s41467-021-27537-5.pdf https://www.nature.com/articles/s41467-021-27537-5 |
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crspringernat:10.1038/s41467-021-27537-5 2023-05-15T16:21:08+02:00 Uppermost crustal structure regulates the flow of the Greenland Ice Sheet Jones, G. A. Ferreira, A. M. G. Kulessa, B. Schimmel, M. Berbellini, A. Morelli, A. Ser Cymru II Program in Low Carbon Energy and the Environment RCUK | Natural Environment Research Council 2021 http://dx.doi.org/10.1038/s41467-021-27537-5 https://www.nature.com/articles/s41467-021-27537-5.pdf https://www.nature.com/articles/s41467-021-27537-5 en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Nature Communications volume 12, issue 1 ISSN 2041-1723 General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry journal-article 2021 crspringernat https://doi.org/10.1038/s41467-021-27537-5 2022-01-04T15:37:37Z Abstract The flow of the Greenland Ice Sheet is controlled by subglacial processes and conditions that depend on the geological provenance and temperature of the crust beneath it, neither of which are adequately known. Here we present a seismic velocity model of the uppermost 5 km of the Greenlandic crust. We show that slow velocities in the upper crust tend to be associated with major outlet glaciers along the ice-sheet margin, and elevated geothermal heat flux along the Iceland hotspot track inland. Outlet glaciers particularly susceptible to basal slip over deformable subglacial sediments include Jakobshavn, Helheim and Kangerdlussuaq, while geothermal warming and softening of basal ice may affect the onset of faster ice flow at Petermann Glacier and the Northeast Greenland Ice Stream. Interactions with the solid earth therefore control the past, present and future dynamics of the Greenland Ice Sheet and must be adequately explored and implemented in ice sheet models. Article in Journal/Newspaper glacier glacier Greenland greenlandic Ice Sheet Iceland Jakobshavn Petermann glacier Springer Nature (via Crossref) Greenland Nature Communications 12 1 |
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Open Polar |
collection |
Springer Nature (via Crossref) |
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crspringernat |
language |
English |
topic |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry |
spellingShingle |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry Jones, G. A. Ferreira, A. M. G. Kulessa, B. Schimmel, M. Berbellini, A. Morelli, A. Uppermost crustal structure regulates the flow of the Greenland Ice Sheet |
topic_facet |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry |
description |
Abstract The flow of the Greenland Ice Sheet is controlled by subglacial processes and conditions that depend on the geological provenance and temperature of the crust beneath it, neither of which are adequately known. Here we present a seismic velocity model of the uppermost 5 km of the Greenlandic crust. We show that slow velocities in the upper crust tend to be associated with major outlet glaciers along the ice-sheet margin, and elevated geothermal heat flux along the Iceland hotspot track inland. Outlet glaciers particularly susceptible to basal slip over deformable subglacial sediments include Jakobshavn, Helheim and Kangerdlussuaq, while geothermal warming and softening of basal ice may affect the onset of faster ice flow at Petermann Glacier and the Northeast Greenland Ice Stream. Interactions with the solid earth therefore control the past, present and future dynamics of the Greenland Ice Sheet and must be adequately explored and implemented in ice sheet models. |
author2 |
Ser Cymru II Program in Low Carbon Energy and the Environment RCUK | Natural Environment Research Council |
format |
Article in Journal/Newspaper |
author |
Jones, G. A. Ferreira, A. M. G. Kulessa, B. Schimmel, M. Berbellini, A. Morelli, A. |
author_facet |
Jones, G. A. Ferreira, A. M. G. Kulessa, B. Schimmel, M. Berbellini, A. Morelli, A. |
author_sort |
Jones, G. A. |
title |
Uppermost crustal structure regulates the flow of the Greenland Ice Sheet |
title_short |
Uppermost crustal structure regulates the flow of the Greenland Ice Sheet |
title_full |
Uppermost crustal structure regulates the flow of the Greenland Ice Sheet |
title_fullStr |
Uppermost crustal structure regulates the flow of the Greenland Ice Sheet |
title_full_unstemmed |
Uppermost crustal structure regulates the flow of the Greenland Ice Sheet |
title_sort |
uppermost crustal structure regulates the flow of the greenland ice sheet |
publisher |
Springer Science and Business Media LLC |
publishDate |
2021 |
url |
http://dx.doi.org/10.1038/s41467-021-27537-5 https://www.nature.com/articles/s41467-021-27537-5.pdf https://www.nature.com/articles/s41467-021-27537-5 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier glacier Greenland greenlandic Ice Sheet Iceland Jakobshavn Petermann glacier |
genre_facet |
glacier glacier Greenland greenlandic Ice Sheet Iceland Jakobshavn Petermann glacier |
op_source |
Nature Communications volume 12, issue 1 ISSN 2041-1723 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41467-021-27537-5 |
container_title |
Nature Communications |
container_volume |
12 |
container_issue |
1 |
_version_ |
1766009159457701888 |